999 resultados para GRAND-CANYON
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Collection : Archives de la linguistique française ; 61
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Collection : Archives de la linguistique française ; 321
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Collection : Archives de la linguistique française ; 160
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O carvão ativado possui a propriedade de adsorver os compostos fenólicos liberados pela oxidação dos tecidos lesionados durante o cultivo in vitro. O objetivo deste trabalho foi avaliar os efeitos da interação entre o carvão ativado e diferentes concentrações de N6-benzilaminopurina (BAP) na multiplicação in vitro da bananeira, cv. Grande Naine (AAA). O meio de cultura utilizado foi o MS, solidificado com 5 g.L-1 de ágar. O cultivo foi mantido em sala de crescimento a 25±2ºC, fotoperíodo de 16 horas e intensidade luminosa de 30 mmol.m-2s-1. Foram avaliadas a presença e a ausência de carvão ativado (0 e 3 g.L-1) e quatro concentrações de BAP (0; 2; 4 e 6 mg.L-1) no meio de cultura. O delineamento foi inteiramente casualizado, com cinco repetições, em um sistema fatorial 2x4. Os explantes foram avaliados a cada 30 dias, por um período de quatro subcultivos. Após cada subcultivo, o comprimento de brotações, a taxa de multiplicação, o vigor, o nível de oxidação das brotações emitidas e o número de raízes formadas foram avaliados. Independentemente das concentrações de BAP, o carvão ativado influenciou significativamente em todas as variáveis analisadas. De maneira geral, a adição de carvão ativado afetou negativamente a taxa de multiplicação, embora tenha melhorado o vigor e o número de raízes e diminuído a oxidação dos explantes. Na ausência de carvão ativado, o BAP proporcionou as maiores taxas de multiplicação das brotações.
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In this paper, we present a computer simulation study of the ion binding process at an ionizable surface using a semi-grand canonical Monte Carlo method that models the surface as a discrete distribution of charged and neutral functional groups in equilibrium with explicit ions modelled in the context of the primitive model. The parameters of the simulation model were tuned and checked by comparison with experimental titrations of carboxylated latex particles in the presence of different ionic strengths of monovalent ions. The titration of these particles was analysed by calculating the degree of dissociation of the latex functional groups vs. pH curves at different background salt concentrations. As the charge of the titrated surface changes during the simulation, a procedure to keep the electroneutrality of the system is required. Here, two approaches are used with the choice depending on the ion selected to maintain electroneutrality: counterion or coion procedures. We compare and discuss the difference between the procedures. The simulations also provided a microscopic description of the electrostatic double layer (EDL) structure as a function of pH and ionic strength. The results allow us to quantify the effect of the size of the background salt ions and of the surface functional groups on the degree of dissociation. The non-homogeneous structure of the EDL was revealed by plotting the counterion density profiles around charged and neutral surface functional groups. © 2011 American Institute of Physics.
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Submarine canyons are sites of intense energy and material exchange between the shelf and the deep adjacent basins. To test the hypothesis that active submarine canyons represent preferential conduits of available food for the deep-sea benthos, two mooring lines were deployed at 1200 m depth from November 2008 to November 2009 inside the Blanes canyon and on the adjacent open slope (Catalan Margin, NW Mediterranean Sea). We investigated the fluxes, biochemical composition and food quality of sinking organic carbon (OC). OC fluxes in the canyon and the open slope varied among sampling periods, though not onsistently in the two sites. In particular, while in the open slope the highest OC fluxes were observed in August 2009, in the canyon the highest OC fluxes occurred in April-May 2009. For almost the entire study period, the OC fluxes in the canyon were significantly higher than those in the open slope, whereas OC contents of sinking particles collected in the open slope were consistently higher than those in the canyon. This result confirms that submarine canyons are effective conveyors of OC to the deep sea. Particles transferred to the deep sea floor through the canyons are predominantly of inorganic origin, significantly higher than that reaching the open slope at a similar water depth. Using multivariate statistical tests, two major clusters of sampling periods were identified: one in the canyon that grouped trap samples collected in December 2008, oncurrently with the occurrence of a major storm at the sea surface, and associated with increased fluxes of nutritionally available particles from the upper shelf. Another cluster grouped samples from both the canyon and the open slope collected in March 2009, concurrently with the occurrence of the seasonal phytoplankton bloom at the sea surface, and associated with increased fluxes of total phytopigments. Our results confirm the key ecological role of submarine canyons for the functioning of deep-sea ecosystems, and highlight the importance of canyons in linking episodic storms and primary production occurring at the sea surface to the deep sea floor.